Horizontal ice flow impacts the firn structure of Greenland's percolation zone
One-dimensional simulations of firn evolution neglect horizontal advection from ice flow, which transports the firn column across climate gradients as it is buried by accumulation. Using a suite of model runs, we demonstrate the impacts of horizontal advection on the development of firn density, tem...
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ftdoajarticles:oai:doaj.org/article:67b78a7e014b4f57b3fc3f5026cc9722 2023-05-15T16:28:15+02:00 Horizontal ice flow impacts the firn structure of Greenland's percolation zone R. Leone J. Harper T. Meierbachtol N. Humphrey 2020-05-01T00:00:00Z https://doi.org/10.5194/tc-14-1703-2020 https://doaj.org/article/67b78a7e014b4f57b3fc3f5026cc9722 EN eng Copernicus Publications https://www.the-cryosphere.net/14/1703/2020/tc-14-1703-2020.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-14-1703-2020 1994-0416 1994-0424 https://doaj.org/article/67b78a7e014b4f57b3fc3f5026cc9722 The Cryosphere, Vol 14, Pp 1703-1712 (2020) Environmental sciences GE1-350 Geology QE1-996.5 article 2020 ftdoajarticles https://doi.org/10.5194/tc-14-1703-2020 2022-12-31T08:54:19Z One-dimensional simulations of firn evolution neglect horizontal advection from ice flow, which transports the firn column across climate gradients as it is buried by accumulation. Using a suite of model runs, we demonstrate the impacts of horizontal advection on the development of firn density, temperature, and the stratigraphy of melt features through the Greenland ice sheet percolation zone. The simulations isolate processes in synthetic runs and investigate four specific transects and an ice core site. Relative to one-dimensional simulations, the horizontal advection process tends to increase the pore close-off depth, reduce the heat content, and decrease the frequency of melt features with depth by emplacing firn sourced from higher locations under increasingly warm and melt-affected surface conditions. Preservation of the advected pore space and cold content is strongly dependent upon the depth of meltwater infiltration. Horizontal ice flow interacts with topography, climate gradients, and meltwater infiltration to influence the evolution of the firn column structure; the interaction between these variables modulates the impact of horizontal advection on firn at locations around Greenland. Pore close-off and firn temperature are mainly impacted in the lowermost 20–30 km of the percolation zone, which may be relevant to migration of the lower percolation zone. Relatively high in the percolation zone, however, the stratigraphy of melt features can have an advection-derived component that should not be conflated with changing climate. Article in Journal/Newspaper Greenland ice core Ice Sheet The Cryosphere Directory of Open Access Journals: DOAJ Articles Greenland The Cryosphere 14 5 1703 1712 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Environmental sciences GE1-350 Geology QE1-996.5 |
spellingShingle |
Environmental sciences GE1-350 Geology QE1-996.5 R. Leone J. Harper T. Meierbachtol N. Humphrey Horizontal ice flow impacts the firn structure of Greenland's percolation zone |
topic_facet |
Environmental sciences GE1-350 Geology QE1-996.5 |
description |
One-dimensional simulations of firn evolution neglect horizontal advection from ice flow, which transports the firn column across climate gradients as it is buried by accumulation. Using a suite of model runs, we demonstrate the impacts of horizontal advection on the development of firn density, temperature, and the stratigraphy of melt features through the Greenland ice sheet percolation zone. The simulations isolate processes in synthetic runs and investigate four specific transects and an ice core site. Relative to one-dimensional simulations, the horizontal advection process tends to increase the pore close-off depth, reduce the heat content, and decrease the frequency of melt features with depth by emplacing firn sourced from higher locations under increasingly warm and melt-affected surface conditions. Preservation of the advected pore space and cold content is strongly dependent upon the depth of meltwater infiltration. Horizontal ice flow interacts with topography, climate gradients, and meltwater infiltration to influence the evolution of the firn column structure; the interaction between these variables modulates the impact of horizontal advection on firn at locations around Greenland. Pore close-off and firn temperature are mainly impacted in the lowermost 20–30 km of the percolation zone, which may be relevant to migration of the lower percolation zone. Relatively high in the percolation zone, however, the stratigraphy of melt features can have an advection-derived component that should not be conflated with changing climate. |
format |
Article in Journal/Newspaper |
author |
R. Leone J. Harper T. Meierbachtol N. Humphrey |
author_facet |
R. Leone J. Harper T. Meierbachtol N. Humphrey |
author_sort |
R. Leone |
title |
Horizontal ice flow impacts the firn structure of Greenland's percolation zone |
title_short |
Horizontal ice flow impacts the firn structure of Greenland's percolation zone |
title_full |
Horizontal ice flow impacts the firn structure of Greenland's percolation zone |
title_fullStr |
Horizontal ice flow impacts the firn structure of Greenland's percolation zone |
title_full_unstemmed |
Horizontal ice flow impacts the firn structure of Greenland's percolation zone |
title_sort |
horizontal ice flow impacts the firn structure of greenland's percolation zone |
publisher |
Copernicus Publications |
publishDate |
2020 |
url |
https://doi.org/10.5194/tc-14-1703-2020 https://doaj.org/article/67b78a7e014b4f57b3fc3f5026cc9722 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland ice core Ice Sheet The Cryosphere |
genre_facet |
Greenland ice core Ice Sheet The Cryosphere |
op_source |
The Cryosphere, Vol 14, Pp 1703-1712 (2020) |
op_relation |
https://www.the-cryosphere.net/14/1703/2020/tc-14-1703-2020.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-14-1703-2020 1994-0416 1994-0424 https://doaj.org/article/67b78a7e014b4f57b3fc3f5026cc9722 |
op_doi |
https://doi.org/10.5194/tc-14-1703-2020 |
container_title |
The Cryosphere |
container_volume |
14 |
container_issue |
5 |
container_start_page |
1703 |
op_container_end_page |
1712 |
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1766017879207051264 |